Vertical and horizontal surface waves are both types of seismic waves that travel along the Earth's surface. They are both considered to be surface waves, which means they do not penetrate deep into the Earth like body waves. These waves are typically the most destructive during an earthquake due to their ability to cause significant ground shaking and damage.
It depends (IS) the frequency of the waves.
Ripple.
Count the number of waves passing a point in one second. That is frequency. Or count waves for 10 seconds and divide by 10.
It depends on the objects, how far apart they are and whether or not one can be seen from the other. If they are moderately far apart, echo location (sonar or radar) located at one of the objects can be used. A beam of radio or sound waves is aimed at the object and the time taken to receive an echo is measured. Since the speed of radio waves or sound waves in the relevant medium is known, the distance travelled by these waves can be calculated. The distance to the object is then half the calculated distance (the waves have to go there and come back).
Comparison of waves going through the solid inner core and those just skimming it can show the rotation of the inner core.
Surface waves consist of two main types: Rayleigh waves and Love waves. Rayleigh waves move in an elliptical motion with both vertical and horizontal components, causing ground particles to move in an elliptical path. Love waves, on the other hand, only have horizontal motion and do not involve vertical movement of the ground particles.
Simple answer:When a stone is thrown into quiet water, the circular waves that are formed are transverse waves. We say the waves are circular because the shape of the wave front is circular and we say it is transverse because the surface disturbance is vertical, perpendicular plane of the surface in which the wave moves.The waves have both properties of being circular and transverse.More Explanation:Transverse waves are waves where the direction of the oscillatory motion is perpendicular to the direction of propagation of the wave.The waves on the surface of water are a vertical motion of the water.The waves on the surface move on the surface, which is horizontal, so the propagation is in the horizontal direction.Horizontal is perpendicular to vertical, so circular water waves as well as linear water waves are transverse. Indeed, no matter what peculiar shape you produce, the water disturbance is vertical and the motion of propagation is restricted to the horizontal surface.
body waves and surface waves
Love waves are a type of surface seismic wave that cause horizontal movement during an earthquake, primarily responsible for horizontal ground shaking. Raleigh waves are another type of surface seismic wave that cause vertical movement during an earthquake, resulting in vertical ground shaking. Both wave types travel along the Earth's surface and can cause significant damage to structures.
The subtypes of secondary waves (S-waves) are Love waves and Rayleigh waves. Love waves cause horizontal movement, while Rayleigh waves cause both horizontal and vertical movement. Both types of waves are surface waves that move along the Earth's crust.
The biggest seismic waves are surface waves, which travel along the Earth's surface and are usually the most destructive during an earthquake. The two main types of surface waves are Rayleigh waves and Love waves. Rayleigh waves cause the ground to move elliptically in vertical and horizontal directions, while Love waves cause horizontal shearing motion.
Examples of surface waves include ocean waves, ripples on water, and ground waves that travel along the Earth's surface during an earthquake. These waves involve both vertical and horizontal motion at the boundary between mediums, such as air and water or air and land.
Surface waves, also known as Love waves and Rayleigh waves, travel only across the surface of the Earth. They have horizontal and vertical motion that can cause significant damage during an earthquake. These waves are slower than body waves but have larger amplitudes.
The glare that reflects from a horizontal surface is horizontally polarized, meaning the light waves are mostly oscillating in a horizontal plane. This polarization causes the glare to be more intense when viewed horizontally.
Love waves are surface waves that move in a horizontal, side-to-side motion, while Rayleigh waves have a rolling motion that combines both vertical and horizontal movement. Rayleigh waves travel slower than Love waves and are more destructive in causing ground movement during an earthquake. Love waves only travel on the surface, while Rayleigh waves travel both on the surface and through the interior of the Earth.
A Love wave is a type of surface seismic wave that causes horizontal shearing of the ground in a vertical plane. It moves in a horizontal, elliptical motion perpendicular to the direction of wave propagation. Love waves are more destructive than other surface waves and travel faster than Rayleigh waves.
Light acts like both a particle and a wave. These particle-waves are oriented in random directions. Polarisation filters basically filter out the randomly oriented waves, and ensure that only light that is 'polarized' in a certain direction can pass through.Horizontal polarisation is when the light waves are oriented horizontally, and vertical is when the waves are vertical. The same princaple applies to the whole EM spectrum.